On the geometry of aggregate snowflakes
Axel Seifert, Christoph Siewert, Fabian Jakub, Leonie von Terzi, Stefan Kneifel
TL;DR
This work addresses the mismatch between traditional, mean-geometry snowflake representations and the actual wide variability of aggregate snowflakes by developing a physics-based, stochastic parameterization of aggregate geometry. It generates millions of synthetic aggregates from a detailed 3D aggregation model and derives joint distributions for the key geometric descriptors ${D}_\text{norm}$, ${\phi}$, and $q$, which are then integrated into a Lagrangian particle framework as pseudo-prognostic variables. The approach demonstrates that a lognormal description of ${D}_\text{norm}$, together with habit-dependent parameterizations for ${D}_\text{max}$, ${\phi}$, and $q$, captures essential variability, modestly increases ensemble fall speeds, enhances aggregation, and broadens radar signatures in forward-model simulations. The results offer a path toward more realistic ice microphysics in weather and climate models and improved interpretation of multi-frequency radar observations, while highlighting the need for memory effects, habit-dependent sticking, and observational validation in future work.
Abstract
Snowflakes play a crucial role in weather and climate. A significant portion of precipitation that reaches the surface originates as ice, even when it ultimately falls as rain. Contrary to the popular image of symmetric, dendritic crystals, most large snowflakes are irregular aggregates formed through the collision of primary ice crystals, such as hexagonal plates, columns, and dendrites. These aggregates exhibit complex, fractal-like structures, particularly at large sizes. Despite this structural complexity, each aggregate snowflake is unique, with properties that vary significantly around the mean - variability that is typically neglected in weather and climate models. Using a physically based aggregation model, we generate millions of synthetic snowflakes to investigate their geometric properties. The resulting dataset reveals that, for a given monomer number (cluster size) and mass, the maximum dimension follows approximately a lognormal distribution. We present a parameterization of aggregate geometry that captures key statistical properties, including maximum dimension, aspect ratio, cross-sectional area, and their joint correlations. This formulation enables a stochastic representation of aggregate snowflakes in Lagrangian particle models. Incorporating this variability improves the realism of simulated fall velocities, enhances growth rates by aggregation, and broadens Doppler radar spectra in closer agreement with observations.
